Exploring the mechanisms of Devonian oceanic anoxia: impact of ocean dynamics, palaeogeography, and orbital forcing

<p>The Devonian is a warmer-than-present geological period spanning from 419 to 359 million years ago (Ma) characterized by multiple identified ocean anoxic/hypoxic events. Despite decades of extensive investigation, no consensus has been reached regarding the drivers of these anoxic events....

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Bibliographic Details
Main Authors: J. Gérard, L. Sablon, J. J. C. Huygh, A.-C. Da Silva, A. Pohl, C. Vérard, M. Crucifix
Format: Article
Language:English
Published: Copernicus Publications 2025-01-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/21/239/2025/cp-21-239-2025.pdf
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